Sink: Atmosphere V(t)
Source: Rain or
Irrigation
Leaves
Water Vapor
"Crown"
Stem
Soil Surface
Transpiration
Water Stress
s1
r1
LAI
Absorbing
Plant Water
s2
Roots r2
Rain/Irrigation
Root Length
Root Uptake
Resistance
si
Potential Gradient
ri
Soil Water
Bottom of Root Zone
Matric Potential
sn
H2O
Figure 5. A root system in layered soil viewed as a
Figure 6. Water flow in the soilroot continuum. The
resistance network. Water held in capacitors moves
"valve" symbols represent water flow rates between
rectangular storage compartments or to external "sink"
roots but not from roots into the soil (after Hillel 1977).
in the atmosphere or groundwater (after Huck and Hillel
1983).
Table 3. Plant resistance, Rp, data of various crops extracted from litera-
ture (after Feddes 1981).
Type of
Root depth
Rp
(103 cm)
Crop
experiment
(cm)
Source
Birds foot trefoil
Lab
60
11.2
Gardner and Ehlig (1962)
Grass
Field
26
10.4
Rijtema (1965)
Potatoes
Field
40
10.3
Endrodi and Rijtema (1969)
Red cabbage
Field
4282
31.436.3
Feddes (1971)
Wheat
Lab
45
921
Yang and de Jong (1971)
Wheat
Lab
18
3158
Yang and de Jong (1972)
Italian ryegrass
Lab
22
517.5
Hansen (1974)
Maize
Greenhouse
--
13
Reicosky and Ritchie (1976)
Grain sorghum
Field
100
11
Reicosky and Ritchie (1976)
Douglas fir
Field
80
25
Nnyamah (1977)
lished literature that measurement of resistances
change to vapor and diffuses through the stomata
encountered in the soilrootplant system is still
and the leaf/air boundary layer. A generalized
difficult or even impossible for many crops.
overview of macroscopic water flow processes is
The pathway of water movement is from bulk
illustrated in Figure 6. Numerous water uptake
soil to the rhizosphere, across the rhizosphere
models are published in the literature and can be
and the soil/root interface, across the cortex and
classified as "macroscopic" or "microscopic."
the endodermis, and then into the lumen of the
xylem. Water then moves along the xylem to the
Macroscopic models
substomatal cavities where it undergoes a phase
Macroscopic models assume the vertical tran-
6